Figure 1 shows images of differently illuminated Mondrian patterns used in the experiment. The patterns consisted of 49 (7 × 7) abutting, 1°-visual-angle square, uniform, simulated Lambertian surfaces with spectral reflectances drawn at random from either the 1269 samples in the
Munsell Book of Color 22,29 (
Fig. 1, top row) or from 5,379,200 (=820 × 820 × 8) samples in eight hyperspectral images of four urban natural scenes and of four rural natural scenes (
Fig. 1, bottom row), each measuring 820 × 820 pixels.
30 Because reflectances were sampled uniformly, the distribution of colors in the patterns of natural spectra reproduced their natural relative abundances.
The images were generated on the screen of a computer-controlled color monitor (for normal trichromats, the degree of color constancy depends little on whether simulated or real surfaces are used as stimuli). The monitor RGB calculations were based on the appropriate color-matching functions for each group of subjects. For the dichromats and normal trichromats, the Smith and Pokorny
31 normal cone fundamentals were used. For the protanomalous and deuteranomalous trichromats, Rayleigh match midpoints fell largely into separate groups, and the DeMarco et al.
32 calculations for average pigments in anomalous trichromacy were therefore used. Spectra were sampled at 10-nm intervals, and integrations were performed over 400 to 720 nm.
30
In each trial, two images of a single pattern were presented in successive 1-second intervals, with no intervening gap, to avoid involving memory.
33 In the first interval, the pattern appeared illuminated by the first global illuminant, a fixed, spatially uniform daylight that was either bluish, of correlated color temperature 25,000 K (
Fig. 1, left column), or yellowish, of correlated color temperature 4000 K (not shown). In the second interval, the pattern made from the same reflecting surfaces appeared illuminated by the second global illuminant, a fixed, spatially uniform, whitish daylight of correlated color temperature 6700 K (
Fig. 1, right column), except for the center surface, in which 6700 K daylight was replaced by a spatially uniform local illuminant constructed from a linear combination of the daylight spectral basis functions.
34 The effect of the local illuminant was to simulate a reflectance change in the center surface. That it was based on a linear approximation was only for computational convenience and had no theoretical relevance. The chromaticity of the local illuminant was sampled randomly in each trial from a large convex gamut in the CIE 1976 (
u′
, v′) diagram consisting of 65 locations, shown by the small solid points in
Figures 2 and
3. Further details of the experimental stimuli, apparatus, and calibration have been published elsewhere.
28